Caledonite is a striking lead-copper sulfate-carbonate mineral known for its vibrant deep blue-green to teal color. It is most frequently found as small, distinct prismatic crystals or crusts in the oxidized zones of lead-copper ore deposits, often associated with linarite.
Is this caledonite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch caledonite with a known reference. Caledonite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: blue, blue green, green, dark green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic, radial, striated.
Often confused with
Caledonite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside caledonite
Minerals reported to co-occur with caledonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂Pb₅(SO₄)₃(CO₃)(OH)₆
- Mohs hardness
- 2.5-3
- Density
- 5.6-5.76 g/cm³
- Streak
- Pale green
- Luster
- Vitreous to resinous
- Transparency
- Translucent to transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic, radial, striated
- Cleavage
- On {010}, perfect; on {100} and {101}, imperfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An uncommon secondary mineral in the oxidized portions of Pb–Cu deposits
Where rockhounds find caledonite
Classic worldwide localities
- Mammoth-St. Anthony mine, Tiger, Pinal Co., in the Rowley mine, near Theba, Maricopa Co., Arizona, USA
- Mex-Tex mine, near Bingham, Hansonburg district, Socorro Co., New Mexico, USA
- Blue Bell mine, near Baker, San Bernardino Co., at the Chance mine, Chidago Canyon, Mono Co., and from Cerro Gordo, Inyo Co., California, USA
- Leadhills, Lanarkshire, and Wanlockhead, Dumfriesshire, Scotland
- Red Gill and other mines, Caldbeck Fells, Cumbria, England
- Preobrazhensky mine, Beresovsk, near Yekaterinburg (Sverdlovsk), Middle Ural Mountains, Russia
Field-hunting tip
Where it forms: An uncommon secondary mineral in the oxidized portions of Pb–Cu deposits. If you start seeing cerussite, anglesite, leadhillite in float, you are in the right ground. Typical habit: prismatic, radial, striated. Train your eye for that shape before scanning the outcrop.







